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GUUS VAN DE GEER

Biographic Data

ID5234565
NAMEGUUS VAN DE GEER
GIVEN NAMESGUUS
FAMILY NAMEVAN DE GEER
SIGNATUREVAN DE GEER G
VERIFIEDNo
TOTAL WORKS1
TOTAL CITATIONS2
WORKS AS AUTHOR1
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1991
LATEST PUBLICATION YEAR1991
H-INDEX1
  • Late Glacial and Holocene Vegetation History at Dublin Bog North‐Central Tasmania

    Open Access•Eric A Colhoun, GUUS VAN DE GEER et al.•ARTICLE•Australian Geographical Studies•1991•Cited by: 2•References: 14

    Percentage and influx pollen analyses of a 9.17 m core from Dublin Bog give a post last glaciation vegetation history (‐13.6 to 0 ka BP) for the upper Mersey Valley. Herbaceous vegetation of Gramineae, Compositae and Chenopodiaceae developed rapidly after deglaciation and lasted until 13.2 ka BP. Around 13 ka BP Eucalyptus woodland and forest developed rapidly on the valley floor. At the same time Pomaderris apetala became an important understore…

  • Late Glacial and Holocene Vegetation History at Dublin Bog North‐Central Tasmania

    Open Access•Eric A Colhoun, GUUS VAN DE GEER et al.•ARTICLE•Australian Geographical Studies•1991•Cited by: 2•References: 14

    Percentage and influx pollen analyses of a 9.17 m core from Dublin Bog give a post last glaciation vegetation history (‐13.6 to 0 ka BP) for the upper Mersey Valley. Herbaceous vegetation of Gramineae, Compositae and Chenopodiaceae developed rapidly after deglaciation and lasted until 13.2 ka BP. Around 13 ka BP Eucalyptus woodland and forest developed rapidly on the valley floor. At the same time Pomaderris apetala became an important understore…

  • Late Glacial and Holocene Vegetation History at Dublin Bog North‐Central Tasmania

    Open Access•Eric A Colhoun, GUUS VAN DE GEER et al.•ARTICLE•Australian Geographical Studies•1991•Cited by: 2•References: 14

    Percentage and influx pollen analyses of a 9.17 m core from Dublin Bog give a post last glaciation vegetation history (‐13.6 to 0 ka BP) for the upper Mersey Valley. Herbaceous vegetation of Gramineae, Compositae and Chenopodiaceae developed rapidly after deglaciation and lasted until 13.2 ka BP. Around 13 ka BP Eucalyptus woodland and forest developed rapidly on the valley floor. At the same time Pomaderris apetala became an important understore…

Archaeology (1 work) · Biology (1 work) · Bog (1 work) · Deglaciation (1 work) · Ecology (1 work) · Ecology (1 work) · Ecology and Vegetation Dynamics Studies (1 work) · Geography (1 work) · Geology (1 work) · Geology (1 work)

Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae